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Titlebook: Ecology of a Glacial Flood Plain; J. V. Ward (former Head of Limnology),U. Uehlinger Book 2003 Springer Science+Business Media Dordrecht 2

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发表于 2025-3-21 18:31:02 | 显示全部楼层 |阅读模式
书目名称Ecology of a Glacial Flood Plain
编辑J. V. Ward (former Head of Limnology),U. Uehlinger
视频video
概述Provides an important baseline foundation for examination of the extent and rapidity of impending changes
丛书名称Aquatic Ecology Series
图书封面Titlebook: Ecology of a Glacial Flood Plain;  J. V. Ward (former Head of Limnology),U. Uehlinger Book 2003 Springer Science+Business Media Dordrecht 2
描述This book is a monograph reporting the major findings from a comprehensive study of a glacial flood plain in the Swiss Alps, based on an intensive research program conducted year-round over several years. Until recently, very little was known regarding the ecology of glacial streams. Previous studies typically focused on one or a few aspects and were limited to the summer period. Moreover, this is the first ecological study of a glacial flood plain with a dynamic, multi-thread channel network. Year-round sampling of a system with a complex channel network spawned unanticipated results and new insights into the ecology of glacial streams. The book begins with the landscape features, glacial history, and floodplain evolution of the Val Roseg. This is followed by chapters on channel typology, groundwater-surfacewater interactions, thermal heterogeneity, and nutrient dynamics. Chapters on the biota deal with terrestrial and aquatic flora, hyphomycete fungi, surface zoobenthos, and the interstitial fauna. Functional processes are addressed in chapters on organic matter dynamics, litter decomposition, nutrient limitation, and drift and colonization patterns. The final chapter provides a
出版日期Book 2003
关键词Ecology; Fauna; Flora; ecosystem; ecosystems; seasonal dynamics; temporal dynamics; vegetation
版次1
doihttps://doi.org/10.1007/978-94-017-0181-5
isbn_softcover978-90-481-6507-0
isbn_ebook978-94-017-0181-5Series ISSN 1573-4595 Series E-ISSN 2543-005X
issn_series 1573-4595
copyrightSpringer Science+Business Media Dordrecht 2003
The information of publication is updating

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Groundwater-Surface Water Interactions,cal reservoirs of the catchment including ice, snow, and ground water. An alternative view is to look at streams as “part of the catchment’s downvalley and downgradient transport of water and solutes” (Bencala, 1993). From this perspective, water is transported through the catchment by overland, sur
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Terrestrial Floodplain Vegetation,ng the method of space-for-time substitution (Matthews, 1992). Investigations of the foreland vegetation in the Bernina massif included several studies (Burga, 1999; Flütsch, 1930; Lüdi, 1958; Richter, 1994; Rübel, 1912).
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Interstitial Fauna,(Füreder, 1999; Milner et al., 2000, 2001; Lods-Crozet et al. 2001). Ecological research conducted on 7 streams distributed across Europe, from the French Pyrenees to the arctic archipelago of Svalbard, provided insight into the factors affecting the composition and distribution of benthic invertebr
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Organic Matter Dynamics,tochthonous primary production in the wetted channel and allochthonous inputs of organic detritus produced on the flood plains and uplands. The relative importance of autochthonous versus allochthonous production varies significantly along the river continuum as well as across geographical regions a
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